Modeling of magnetic hysteresis parameters in foraminiferal shells of the Mid-Atlantic Ridge

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Abstract

The composition and magnetic properties of foraminifers from bottom sediments of the Mid-Atlantic Ridge and their artificial analogues obtained by hydrothermal synthesis have been studied. The presence of magnetic hysteresis and theoretical modeling of hysteresis characteristics made it possible to assume the presence of grains of nonstoichiometric magnetite in single and low-domain states.

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About the authors

E. S. Sergienko

Saint Petersburg University

Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 199034

S. Y. Janson

Saint Petersburg University

Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 199034

K. G. Gareev

Saint Petersburg Electrotechnical University “LETI”

Author for correspondence.
Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 197022

P. V. Kharitonskii

Ioffe Institute

Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 194021

A. Yu. Ralin

Far Eastern Federal University

Email: kggareev@etu.ru
Russian Federation, Vladivostok, 690922

T. S. Sheidaev

Saint Petersburg Electrotechnical University “LETI”

Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 197022

E. A. Setrov

Saint Petersburg Electrotechnical University “LETI”

Email: kggareev@etu.ru
Russian Federation, St. Petersburg, 197022

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2. Fig. 1. Optical images of foraminifera samples: F1 – Globorotalia menardii (a), F2 – Orbulina universa (b), Fs1 – Globorotalia menardii (c), Fs2 – Orbulina universa (d), Fs3 – Globigerinoides conglobatus (d), Fart – Orbulina universa (e).

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3. Fig. 2. Hysteresis loops in a field less than 1 T and demagnetization curves by a reverse field: sample F1 (a), F2 (b), Fs1 (c), Fs2 (d), Fs3 (d), Fart (e). The saturation magnetization values ​​obtained in a field of 7 T are given in Table 3.

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